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  3. Origin of the Carbonate Sediments in the Wilkins Peak Member of the Lacustrine Green River Formation (Eocene), Wyoming, USA
  1. Home
  2. Publications
  3. Origin of the Carbonate Sediments in the Wilkins Peak Member of the Lacustrine Green River Formation (Eocene), Wyoming, USA

Origin of the Carbonate Sediments in the Wilkins Peak Member of the Lacustrine Green River Formation (Eocene), Wyoming, USA

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  • 24 November 1978
    • book chapter
    • Published by Wiley
    • p. 109-127
    • https://doi.org/10.1002/9781444303698.ch6
Abstract
No abstract available
Keywords
  • DENSE DOLOMITE SURFACE CRUSTS FORMED ON THE EVAPORATIVE MUDFLAT
  • MOUND-SHAPE TRAVERTINE TUFA PRECIPITATED ALONG SPRING-FED STREAMS
  • CALICHE CRUSTS AND CEMENTS FORMED IN THE ALLUVIAL FANS
  • A LARGE ACCUMULATION OF‘PRIMARY’ DOLOMITE
  • EOCENE GREEN RIVER FORMATION
  • DOLOMITE SURFACE CRUSTS

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